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327 - SciELO

327
RIPARIAN VEGETATION AFFECTED BY BANK EROSION IN THE LOWER
SÃO FRANCISCO RIVER, NORTHEASTERN BRAZIL 1
Francisco Sandro Rodrigues Holanda 2, Laura Galvão da Cunha Santos 3, Cícero Marques dos Santos3,
Ana Patrícia Barreto Casado3, Alceu Pedrotti2 and Genésio Tâmara Ribeiro2
ABSTRACT – Changes in the hydrological regime of the Lower São Francisco River, located in Northeastern
Brazil have brought negative environmental impacts, jeopardizing the flora and fauna of a global biodiversity
hotspot, due to implementation of hydroelectric power dams and surface water withdrawal for irrigation in
public and private perimeters. Remnants of the riparian stratum associated to the riverbank destabilization
in six fragments were studied by surveying trees, shrubs, herbs, and aquatic species. The calculation of the
Factor of Safety (FS) was performed in order to understand the riverbank’s stability related to soil texture
and vegetation cover. An overall number of 51 botanic families distributed in 71 genera and 79 species were
recorded, predominantly from the families Mimosaceae, Myrtaceae, and Fabaceae. The fragmented riparian
vegetation is mostly covered by secondary species under a strong anthropogenic impact such as deforestation,
mining and irrigation, with an advanced erosion process in the river margins. Strong species that withstand
the waves present in the river flow are needed to reduce the constant landslides that are mainly responsible
for the river sedimentation and loss of productive lands. A lack of preservation attitude among the local
landholders was identified, and constitutes a continuing threat to the riparian ecosystem biodiversity.
Key words: Floristic survey, riparian vegetation, riverbank destabilization and São Francisco River.
VEGETAÇÃO CILIAR AFETADA PELA EROSÃO NA MARGEM DO BAIXO
SÃO FRANCISCO, NORDESTE DO BRASIL
RESUMO – Mudanças no regime hidrológico no baixo curso do rio São Francisco, localizado na Região
Nordeste do Brasil, trouxeram impactos negativos, como a ameaça à fauna e à flora em um dos 25 “hotspots”
do mundo para a conservação da biodiversidade, em razão da construção de usinas hidroelétricas e retiradas
de água para irrigação em perímetros de irrigação públicos e privados. Foram estudados remanescentes
da vegetação ciliar associados com a desestabilização dos barrancos do rio, em seis fragmentos de mata,
por meio de levantamento florístico e histórico de degradação dos ecossistemas. Foi também realizado o
cálculo do Fator de Segurança (FS), objetivando compreender a estabilidade dos taludes, relacionando
com textura do solo e cobertura vegetal. Foi identificado um número total de 51 famílias botânicas, distribuídas
em 71 gêneros e 79 espécies, predominantemente das famílias Mimosaceae, Myrtaceae e Fabaceae. A fragmentada
vegetação ciliar, predominantemente dominada por espécies secundárias, sofreu forte pressão antropogênica
pelos desmatamentos, mineração e irrigação, sob um avançado processo erosivo nas suas margens. Se faz
necessária a revegetação com espécies que suportam a ação das ondas contra os barrancos, visando reduzir
1
Recebido em 13.02.2004 e aceito para publicação em 25.11.2004.
Universidade Federal de Sergipe, Cidade Universitária Prof. José Aloisio de Campos, Av. Mal. Rondon, s/n, Jardim Rosa
Elze, São Cristovão-SE, 49.100-000, Brazil, E-mail: <[email protected]>.
3
Universidade Federal de Sergipe - Master Course in Environment and Development.
2
Sociedade de Investigações Florestais
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
328
HOLANDA, F.SR. et al.
os constantes desmoronamentos de grandes blocos de terra que caem no canal do rio, responsáveis pelo
assoreamento e pela perda de terras produtivas. Foi identificada a falta de uma atitude de preservação por
parte dos ribeirinhos, constituindo-se em constante ameaça para a biodiversidade dos ecossistemas ripários.
Palavras-chave: Levantamento florístico, vegetação ciliar, desestabilização de taludes e rio São Francisco.
1. INTRODUCTION
The São Francisco River Basin has been subjected
to development policies, mainly the installation of
hydroelectric dams through the river channel and surface
water withdrawal for irrigation of public and private
lands. As a result of the construction of these dams,
land adjacent to floodplain was flooded and the river
flow regime was altered. In the lower São Francisco
River, which borders the states of Sergipe and Alagoas,
in northeastern Brazil (Fig. 1), serious disturbances
in the major extension of the riparian ecosystem along
the river margin has led to riverbank destabilization,
increasing its erosion, stream lateral migration and
sedimentation, which is reflected directly in the numbers
of sand bars. In effect, erosion is commonly caused
by the exposure of soil, due to the loss of vegetation
which covers and protects the riverbank, as reported
by Kageyama et al. (1994). Although soil parameters
and riverbank characteristics are not enough information
for a precise diagnostic of bank instability (HUNT,
1990), a reasonable prediction of the bank ruptures
can be provided by the qualitative evaluations of various
elements influencing the riverbank instability.
Because of the river basin’s vulnerability to erosion
and the unsustainable activities conducted there, the
flora has been the natural resource most rapidly and
easily threatened. Riparian vegetation on the riverbank
has been seriously and continuously deforested because
of roads, hydroelectric power dams construction, urban
occupation, adjacent land use, irrigated agriculture,
livestock grazing, and the extraction of wood and
minerals. Recent studies in the Lower São Francisco
River showed that only 4% of the total edges still have
riparian vegetation, while the other 96% of the river
margin have been threatened and continuously replaced
by pasture/agriculture systems (ZUCON et al., 1996).
Most of these riparian vegetation remnants are
an extension of the Atlantic rain forest, that used to
cover 100 million hectares in the Brazilian Atlantic Coast,
now reduced to isolated patches (FUNDAÇÃO ..., 1999;
PITHER and KELLMAN, 2002). According to Myers
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
et al. (2000), this is an area featuring exceptional
concentrations of endemic species and experiencing
exceptional loss of habitat.
In the state of Sergipe, the Atlantic rain forest,
which includes part of the riparian remnants, is
characterized, mostly by secondary forest (ZUCON
et al., 1996). Currently these fragments are still exposed
to predatory exploitation, caused by fire, wood extraction
and cattle grazing, even though they are considered
“protected by law”. The objective of this work was
to study riparian vegetation remnants threatened by
the current process of bank erosion in the Lower São
Francisco River Basin.
2. MATERIAL AND METHODS
2.1. Study area
This study was carried out on the margins of the
Lower São Francisco River Basin, located in Sergipe
State, Northeastern Brazil, from the Municipality of
Propriá (10º12’S, 36o50’W) through the Municipalities
of Santana do São Francisco (10º18’S, 36o52’W), Neópolis
(10º19’S, 36o34’W), Ilha das Flores (10º26’S, 36o32’W)
to the river estuary, located in the Municipality of Brejo
Grande (10º25’S, 36o07’W) (SERGIPE, 1997) (Fig. 1).
In the State of Sergipe, the lower sub-basin has
a length of 236 km between its northwestern border
and the mouth of the river, covering 37% of the overall
state area, and 1.2% of the overall São Francisco River
Basin. The extension between the Municipality of Propriá
and the river estuary is 80 km long, covering 34.4%
of the lower river basin (SERGIPE, 1997). The estuarine
wetlands located at the mouth of the river in the
Southwestern Atlantic (Border of Sergipe and Alagoas
States) form a particularly important, environmentally
sensitive interface between riverine and marine
ecosystems (FONTES, 2002).
In the studied area a wide variety of soil types
has been identified, such as patches of ustifluvent,
haplustox, and haplustult (HOLANDA 2000), favoring
the development of different ecosystems and providing
329
Riparian vegetation affected by bank erosion in the...
important information on the identification of the
vegetation in each municipality, correlated to the remnants
riparian patches. The annual average temperature is
26oC and rainfall varies from 806 mm to 1200 mm per
year, with a pronounced dry season from September
to February (SEPLAN, 1979).
2.2. Vegetation survey
Six fragments of riparian vegetation were chosen
to be studied, based on local information on the less
disturbed sites, located at Ilha do Aurélio, Morro do
Aracaré, Fazenda Cajuípe, Ilha do Cachimbão, Ilha do
Monte, and Povoado Cabeço. These sites are located
in the municipalities of Propriá, Santana do São Francisco,
Neópolis, Ilha das Flores, and Brejo Grande, respectively.
At these places a floristic survey of trees, shrubs,
herbs, grass, aquatic species, and others was performed,
characterizing fragments of deciduous and semideciduous forest (alluvial semi-deciduous forest). The
forest was sampled in 10 x 50 meters. Each species
was collected, mounted, labeled, and systematically
arranged in a herbarium, as described in Mori et al.
(1989). Plant species data were listed according to the
classification system of Cronquist (1981).
2.3. Historic riparian deforestation survey
In order to obtain relevant information regarding
the past deforestation, a semi-structured questionnaire
was applied according to Trivinos (1995). A group of
260 people was interviewed among fishers, farmers,
landowners, and others, who live in the studied riverine
area. Additionally, information on the five less disturbed
sites in the river margin was collected through the
interview with key informers (PELTO and PELTO, 1978).
The interviewers’ questions were designed to determine
the knowledge of the local population about river margin
changes, related to riparian vegetation deforested species,
and its influence on the river bank erosion over the
years. This population was selected for the survey
because they live and work in that area, and exert a
strong pressure on the natural resources in those
ecosystems. This survey employed a non-random and
non-probalistic assessment data analysis, considering
that the participants responded to questionnaires applied
by the interviewers, who have a previous knowledge
about the sampled population intrinsic characteristics
(LEVIN, 1978).
2.4. River banks stability
Figure 1 – Location of the study area, along the Lower São
Francisco River.
Figura 1 – Localização da área de estudo, no baixo rio São
Francisco.
In order to understand the stability of riverbanks,
three different sites (A, B and C), located in the
Municipality of Propriá (Cotinguiba-Pindoba Irrigated
Perimeter), were selected. These sites were selected
in 1999 (CASADO et al., 2002), based on the presence
and characteristics of their vegetation cover, bank height,
soil particles composition and riverbank erosion stage
process, representing the most common soil type such
as alluvium soils. The chosen sites A, B and C were
mostly covered by grass-shrubs, vegetable crop field
and by grass and scarce trees, respectively, and are
different from the sites where the floristic survey was
perfomed. These essays were arranged in a randomized
block design, with three replications. The estudied
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
330
HOLANDA, F.SR. et al.
sites were basically composed by sand layers
characterized as alluvial soils.
The characteristics of material property strengths
from the soil horizons were achieved by Mohr-Coulomb
material strength criteria for assessing stability, through
the calculation of the Factor of Safety (FS). The FS
is therefore chosen as a ratio of the available shear
strength required to keep the riverbank stable (BURNS,
1999). The data closeness to 1, means stability to the
river slope. The software XSTABL was used to process
data provided by the Bishop/Jambu Method in order
to determine how stable the riverbank is and which
conditions are needed to reactivate these landslides
(SHARMA, 1994), allowing for the calculation of the
FS of a known failure plane.
3 - RESULTS AND DISCUSSION
3.1. Composition of the riparian vegetation remnants
and deforestation
The São Francisco River has a progressive transition
of ecosystems from downstream to upstream, with
mangrove along the sand coastal plain “restinga,” Atlantic
rain forest, Brazilian savanna “cerrado,” and semi-arid
ecosystem “caatinga.” In all sampled sites, replacement
of native species by invading species from the
ecosystems near the riparian zone were noticed, as
previously reported by Rodrigues e Leitão Filho (2000).
This riparian landscape is a mosaic of distinct ecological
formations that works as a corridor, linking different
phyto-ecological regions.
The riverbank in the Ilha do Monte, Municipality
of Ilha das Flores, is mostly covered by aquatic species,
mainly because the original forest was replaced by
coconut. A mosaic of shrubs and small trees from 7
different families were identified such as Araceae,
Gramineae, Hydrocaritaceae, Onagraceae,
Pontederiaceae, Sapindaceae, and Scrophulariaceae,
each one represented by one species (Table 1).
The three following sites: Ilha do Cachimbão, Morro
do Aracaré, and Fazenda Cajuípe have also presented
a great reduction in the number of primary species,
which have been replaced by isolated fragments of
secondary vegetation, considered as invading species.
At Ilha do Cachimbão, a less disturbed riparian
vegetation was found, mostly characterized by a shrubtree stratum. In the central part of this small “island,”
a continuous threat toward the forest devastation has
been correlated to grazing activities, leading to the
observation of only small patches of the riparian forest.
Thus, this fragment was classified into 16 families
distributed in 19 plant species, mainly from the family
Mimosaceae, and native species also identified from
the Atlantic rain forest ecosystem.
Between the river estuary and the Municipality
of Propriá, 51 botanic families distributed in 71 genera
and 79 plant species were identified, predominantly
from the families Mimosaceae, Myrtaceae, and Fabaceae.
Morro do Aracaré still presents an area
predominantly populated by shrubs and scattered trees,
where the overall deforestation was avoided perhaps
due to difficulties in accessibility by the riverine
population, such as the high slope of the hill accessed
only by boat. According to the floristic survey, in this
site 20 different botanic families were found distributed
in 27 plant species predominantly from the family
Mimosaceae (Table 1). Those species were previously
reported by Leitão Filho (1982), as very common in
the Atlantic rain forest.
At Povoado Cabeço located in the river estuary,
Municipality of Brejo Grande, very fragmented riparian
vegetation was found, a consequence of logging by
landholders, leading to an increase in beach and rivermarine erosion. A great number of mangrove trees was
reported, and also an endemic specie of the São Francisco
river estuary such as Craenea sp., called by the local
population “manchica”, (PETROBRAS, 2000). This
species plays a colonizer role in the natural vegetation
succession, commonly established in mangrove’s edge
and in the sand bars. Other species were reported firstly
by Franco (1983), belonging to the sand coastal plain.
In this ecosystem 19 botanic families were found,
distributed in 24 plant species (Table 1).
At Fazenda Cajuípe, the riparian vegetation
deforestation initially occurred because of the expansion
of sugar cane fields (PORTO, 1999), a very common
disturbance and most of the time associated to the Atlantic
forest degradation in Brazil (GASCON et al., 2000), related
to woodcutting to provide fuel for small local sugar cane
mills. Throughout the years, Cocos nucifera (coconut)
has occupied part of this area, because of the suitable
agro ecological conditions. Regardless of the strong
coconut’s presence, the remnant riparian vegetation showed
15 families distributed in 20 different genera and 22 species.
These species were previously reported (FRANCO, 1983)
as being part of different ecosystems such as coastal
plain, Atlantic forest, and “caatinga”.
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
Shrub
Shrub
Laguncularia racemosa Gaert.
6
4
1
6
1 and 4
4
5
5
2 and 4
4
6
6
2 and 3
4
6
6
6
1 and 2
2 and 4
6
Trigoniaceae
Tiliaceae
Ulmaceae
Verbenaceae
Salvinaceae
Scrophulariaceae
Solanaceae
Sapotaceae
Sapindaceae
Rutacea
Rhamnaceae
Rhizophoraceae
Rubiaceae
Pontederiaceae
Poaceae
Nyctaginaceae
Onograceae
Passifloraceae
Piperaceae
Plumbaginaceae
Moraceae
Myrtaceae
Family
Mimosaceae
Liana
Shrub
Tree
Shrub
Aquatic
Herbaceous
Shrub
Shrub
Shrub
Tree
Tree
Tree
Tree
Tree
Tree
Tree
Shrub
Tree
Aquatic
4
2
4
6
2
5
3
6
6
5
1
2
2
4
4
6
4
4
5
2
2 and 3
Aquatic
Aquatic
Bambusa vulgaris Schrader
ex Wendland.
Lasiacis ligulata Hitch
et Chase
Eichornia crassipes
(Water Hyacinth).
Zizyphus joazeiro Mart.
Rizophora mangle L.
Guettarda angelica Mart.
Tocoyena formosa
(Cham. & Schltdl.)
Esenbeckia intermedia
Mart. ex Engl.
Talisia sp.
Talisia sp.
Bumelia satorum
Chrysophyllum marginatum
(Hook.&Arn.) Radlk
Salvinia auriculata Aubl.
Angelonia biflora Benth
Cestrum laevigatum Schletch
Solanum paludosum Moric.
Solanum stipulaceum
Roem. & Schult.
Trigonia sp.
Triumfetta semitriloba Jacq.
Celtis sp.
Lantana camara L.
1
2
4
3 and 4
3
5
4
2
1
Tree
2
2, 3 and 4
2, 3 and 4
4
2 and 3
2
3
4
6
Occurrence
1
Shrub
Myrcia sp1
Myrcia sp2
Shrub
Psidium sp
Tree
Guapira pernambucensis (Casar.) Shrub
Ludwigia octovalvis (Jacq.)
Aquatic
Passiflora sp.
Liana
Piper arboreum Aubl.
Shrub
Plumbago scandens L.
Herbaceous
Campomanesia viatoris Landrum
Specie
Growth habit
Anadenanthera macrocarpa
Tree
(Benth) Brenan
Calliandra depauperata Benth.
Shrub
Inga edulis Mart.
Tree
Inga sp1
Tree
Inga sp2
Tree
Mimosa sp.
Shrub
Pithecelobium sp.
Tree
Ficus eximia Schott
Tree
Eugenia sp1
Shrub
Eugenia sp2
Shrub
1 - Ilha do Aurélio; 2 - Morro do Aracaré; 3 -Ilha do Cachimbão; 4 - Fazenda Cajuípe; 5 - Ilha do Monte e 6 - Povoado Cabeço.
Herbaceous
Aquatic
Shrub
Shrub
Craenea sp.
Lafoensia sp.
Bakeridesia sp.
Byrsonima gardneriana Juss.
Tree
Liana
Shrub
Tree
Andira fraxinifolia enth. Clitoria sp
Clitoria sp.
Dalbergia ecastophyllum (L.) Taub.
Lonchocarpus sericeus (Poiret) Kunth
Lythraceae
Hydrocharitaceae
Malvaceae
Malpighiaceae
Tree
Pera ferruginea (Schott) Mull. Arg.
Tree
Shrub
Herbaceous
Aquatic
Liana
Shrub
Liana
Shrub
Shrub
Wedelia paludosa DC.
Davilla flexuosa St. Hill
Erythroxylum sp.
Croton sp.
Machaerium augustifolium Vog.
Casearia sylvestris Sw.
Andropogon bicornis L.
Elodea sp.
Strutanthus sp.
Shrub
Venonia chalybaea Mart.Ex DC.
1
6
2 and 3
2
6
2 and 3
1 and 6
2
6
2 and 6
Tree
3, 4 and 6
2
4and 6
2, 3 and 6
3,5, and 6
1
6
6
1 and 2
Occurrence
2
Tree
Tree
Tree
Tree
Tree
Tree
Tree
Aquatic
Flacourtiaceae
Gramineae
Hydrocharitaceae
Loranthaceae
Fabaceae
Compositae
Dilleniaceae
Erythroxylaceae
Euphorbiaceae
Combretaceae
Capparaceae
Cecropiaceae
Chrysobalanaceae
Ciperaceae
Caesalpiniaceae
Burseraceae
Bignoniaceae
Annonaceae
Araceae
Aristolochiaceae
Avicenniaceae
Tree
Tree
Tree
Tree
Aquatic
Liana
Tree
Tree
Tree
Anacardium ocidentale L.
Astronium fraxinifolium Schott
Schinus terebenthifolius Raddi
Annona cacans Warm.
Montrichardia linifera Schott
Aristolochia cymbifera Mart.& Zucc.
Avicennia germinans (L) Steam
Avicennia achaweriana Stap & Lechm
Tabebuia impetiginosa
(Mart. Ex DC.) Stand.
Protium heptaphyllum (Aubl.)
Marchand D.Dally
Bauhinia sp.
Cassia macranthera DC. Ex Collad.
Cassia grandis L.f.
Hymenaea sp.
Capparis flexuosa L.
Cecropia pachystachya Trec.
Couepia impressa Prance
Eleocharis elegans (Kunth)
Roem. & Schult
Conocarpus erectus L.
Anacardiaceae
Growth habit
Herbaceous
Specie
Ruellia sp.
Family
Acanthaceae
Table 1 – Species of the riparian vegetation fragments identified at the margin of the Lower São Francisco River Basin in the State of Sergipe State,
northeastern Brazil in December 2000
Tabela 1 – Espécies identificadas em fragmentos da vegetação ciliar, na margem do baixo rio São Francisco, no Estado de Sergipe, Nordeste do Brasil,
em dezembro de 2000
Riparian vegetation affected by bank erosion in the...
331
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
332
At the Ilha do Aurélio the riparian vegetation was
greatly reduced mostly because of anthropogenic
activities, leading to a remarkable bank erosion processes.
Thus, only few riparian fragments were identified,
presenting 10 botanic families distributed in 11 plant
species, some of them invading species from the river’s
basin semi-arid area.
From the river estuary to upstream toward the
Municipality of Propriá, the most broadly distributed
species along the riverbanks were Inga edulis,
Montrichardia linifera and Mimosa sp. Inga edulis
Mart (“ingazeira”) is a semi-deciduous tree, heliophyte,
selective hygrophyla, commonly found in wetlands,
which are mostly occupied by secondary species. It
is also very abundant along margins of large rivers,
developing very fast as pioneer species in secondary
ecological succession. M. linifera (Arruda) Shott
(“aninga”) was also found spread from the Municipality
of Santana do São Francisco until the river estuary.
It is a pioneer species near the mangrove ecosystem
and in the sand bars, characterized as aquatic herbaceous
plant, measuring up to five meters tall and 20 cm or
more in diameter, with straight and fusiform trunk.
Mimosa sp. (“calumbi”) is a nitrogen-fixing shrub, that
colonizes land after clearing or burning. It grows quickly,
providing cover and extra nitrogen to the soil for slower
growing plants. It can be found broadly distributed
from the Municipality of Propriá to the Municipality
of Ilha das Flores.
Other plant species are also very common along
the river margin, such as Bambusa vulgaris (“caniço”),
Eleocharis elegans (“junco”) and Eichornia crassipes
(“balseiro”), mostly covering wetlands, protecting the
riverbank against the force of the water waves. In
agreement with Nilsson et al. (1989), it was noticed
that species like Eleocharis sp. presented dense root
network growth that binds bank sediments and resists
plant removal by flood scour.
3.2. Changes in the riparian vegetation throughout the
years
According to opinions of the riverine population,
the riparian vegetation has been submitted to a very
serious anthropogenic degradation throughout the
years, with a strong shift to a higher density of aquatic
species mainly from the families Hydrocharitaceae and
Scrophulariaceae, such as Elodea sp. (“cabelo”) and
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
HOLANDA, F.SR. et al.
Bacopa myriophylloides (“lodo”), thus now very
common in the river channel. Several people tried to
link the remarkable presence of those aquatic species
to the lack of natural river flooding season, because
the past strong flow used to remove plants from the
main river channel. Also, the absence of sediments
in the clear water released by the electricpower dams,
allows more sunlight to penetrate into the deep river
water. This situation together with the river sedimentation
because of the riverbank erosion, has created favorable
conditions for those fast propagated species. In addition
people also report that body contact with Elodea sp.
irritates the skin of fishers, probably related to the
calcium oxalate produced by this plant, and stongly
contributing to hide fish.
Beyond the above-cited species, strongly spread
in all Lower São Francisco River, a grass called
Andropogon bicornis (“rabo-de-raposa”), also very
common, causes serious navigation problems and
complaints from the local fishers.
A list of plant species previously found in the
river margin according to the local people, included
Inga edulis, Eichornia crassipes, Mimosa sp., Bambusa
vulgaris, Eleocharis elegans and Montrichardia linifera,
as very common in the past years, and still widespread
in the region (Table 2). The presence of Cocos nucifera,
is also very frequent, even though it is mostly found
in the Municipality of Neópolis where its commercial
production is still very common, and in the Municipality
of Brejo Grande, in the sand coastal plain ecosystem,
ecologically favorable to coconut propagation. In both
sites, the plants are widely spaced according to the
current harvest techniques, adding river margin
disturbances. Other species are present in small fragments
patches, explaining the strong loss of genetic biodiversity.
In the riparian vegetation, the density of some
species that were not very common in the past, has
increased. Besides Elodea sp. other species such as
Cassia grandis (“canafístula”), Piper arboreum
(“pipeira”), Laguncularia racemes (“mangue branco”),
and Mangifera indica (“manga”), were frequently cited.
In the mangrove ecosystem an increase in the density
of Inga edulis was noticed. The frequency of certain
species such as Mangifera indica can be explained
by the increase in commercial production mango fields,
located in irrigated areas near the river margin, also
contributing to the riparian vegetation degradation.
333
Riparian vegetation affected by bank erosion in the...
Table 2 – Species of the original riparian cover in the lower São Francisco riverbanks in the State of Sergipe State, northeastern
Brazil, according to the questionaire applied to the local population, in December 2000
Tabela 2 – Espécies da vegetação ciliar original nas margens do baixo Rio São Francisco, Estado de Sergipe, Nordeste
do Brasil, de acordo com o questionário aplicado à população local, em dezembro 2000
Family
Anacardiaceae
Specie
Anacardium ocidentale L.
Anacardiaceae
Mangifera indica L.
Anacardiaceae
Annonaceae
Araceae
Arecaceae
Spondias dulcis Forst.
Annona cacans Warm.
Montrichardia linifera Schott
Cocos nucifera L.
Bignoniaceae
Caesalpiniaceae
Caesalpiniaceae
Cecropiaceae
Chrysobalanaceae
Ciperaceae
Combretaceae
Convolvulaceae
Fabaceae
Flacourtiaceae
Meliaceae
Mimosaceae
Mimosaceae
Moraceae
Myrtaceae
Myrtaceae
Passifloraceae
Piperaceae
Poaceae
Poaceae
Pontederiaceae
Rhamnaceae
Rosaceae
Rubiaceae
Rubiaceae
Rubiaceae
Common Name
Caju
Growth Habit
Tree
Occurrence
1, 3 and 5
Mangueira
Tree
1, 2, 3 and 4
Cajazeira
Araticum
Aninga
Coco, Coconut
Tree
Tree
Aquatic
Tree
3 and 5
5
4
2, 3, 4 and 5
Tabebuia caraiba Mart.
Cassia fistula L.
Craibeira
Canafístula
Tree
Tree
1
1, 2 and 4
Caesalpinea pyramidalis Tull.
Cecropia pachystachya Trec.
Couepia impressa Prance
Eleocharis elegans (Kunth)
Roem. &Schult
Terminalia catalpa L.
Ipomoaea fistulosa Mart.
Dalbergia ecastophyllum (L.)
Casearia sylvestris Sw.
Cedrela fissilis Vell.
Inga edulis Mart.
Mimosa sp.
Ficus eximia Schott
Eugenia sp.
Psidium sp.
Passiflora sp.
Piper arborium Aubl.
Bambusa vulgaris Schrader
ex Wendland.
Oryza sativa L.
Eichornia crassipes (Martius)
Zizyphus joazeiro Mart.
Licania humilis Cham. & Schlecht
Anisomeris sp.
Genipa americana L.
Guettarda angelica Mart.
Catingueira
Umbaúba
Maçãnzeira
Junco
Tree
Tree
Tree
Aquatic
1
4
1
2 and 3
Amendoeira
Mata-cobra
Bugio
Maria-preta
Cedro
Ingazeira
Calumbi
Gameleira
Cambuí
Araçá
Maracujazeiro
Pipeira
Caniço
Tree
Herb
Shrub
Shrub
Tree
Tree
Shrub
Tree
Tree
Shrub
Liana
Strub
Aquatic
1
1
5
5
1
1, 2, 3, 4 and 5
1, 3 and 4
1
5
4 and 5
5
1, 3 and 4
1 and3
Arroz
Balseiro
Joazeiro
Oiti
Espinho branco
Jenipapeiro
Rompe-gibão
Herb
Aquatic
Tree
Tree
Shrub
Tree
Strub
1 and 3
1, 2, 3, 4 and 5
1
5
5
1, 2 and 3
1 and 2
1 – Municipality of Propriá; 2 - Municipality of Santana do São Francisco; 3 - Municipality of Neópolis; 4 - Municipality of Ilha das
Flores; 5 - Municipality of Brejo Grande.
Based on the local population opinions it seems
that Inga edulis, the most frequently mentioned species,
has developed an important role as a river’s margin
protector, followed by Eichornia crassipes and
Montrichardia linifera. It was noticed that those answers
are in accordance with the empirical published data
by Franco (1983). Mimosa sp. has been also used as
a bank protector species by the riverine population,
although this species seems more common in the upper
part of the river. On the other hand, Inga edulis and
Montrichardia linifera were found densely populating
the studied area, offering a good protection to the river
margin.
3.3. River Bank Stability
Casado et al. (2002), reported an ascending
accumulated erosion rate of 8.30 m per year from 1999
to 2001 in site A, while sites B and C had an accumulated
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
334
HOLANDA, F.SR. et al.
rate of 47.3 and 4.45m per year, respectively (Table
3). The three sites studied had different results of Factor
of Safety (FS) related to bank instability, and all were
classified as unstable. Only the site C has presented
FS of 0.975, close to a situation of equilibrium. The
FS used to explain the riverbank stability results, is
the ratio of the available shear strength to the minimum
shear strength needed for equilibrium, explained as
an interactive method. According to this definition
a bank (slope) is unstable when the Factor of Safety
is lower than 1. The FS of 0.975 calculated for site C,
may be explained by its low bank height. In this site
the soil is mostly dominated by silt and clay fractions
and the present vegetation in the bank was predominately
grass and sparse trees. According to Tschebotarioff
(1978), erosion occurs particularly faster in the bank
dominated by silt and very fine sand, which have very
low cohesion.
Because of the very low cohesion forces of the
soil particles in the bank, there is an urgent need of
riverbank stabilization along the river margin. Strong
species that withstand the waves present in the river
are needed to reduce the constant landslides that are
mainly responsible for the river sedimentation and loss
of productive lands. A similar conclusion was reached
for bank stability because the soils are predominantly
alluvial such as haplustult and ustifluvent. These soils
are characterized by variations in resistance to soil
rupture, both vertically and horizontally (SANTOS,
2002). Thus, vegetative protection could help control
the erosion process, even in very vertical and high
Table 3 – Classification of slope stability in the studied sites
(A, B and C) based en the factor of safety (FS), in
the lower São Francisco riverbanks in the State of
Sergipe State, northeastern Brazil, in December 2000
Tabela 3 – Classificação da estabilidade do talude nos sítios
estudados (A, B e C), baseado no fator de segurança
(FS), no baixo rio São Francisco, Estado de Sergipe,
Nordeste do Brasil, em dezembro 2000
Site
A
B
C
Bank mean
Height (m)*
5.21
6.36
3.91
Erosion Rate
(m per year)
8.30
47.30
4.45
FS**
Slope
Stability***
0.463
Unstable
0.663
Unstable
0.975
Unstable
Adapted from Casado et al. (2002).
*Measured from the base (river water level) to the botton (soil surface).
** FS ≥ 1, means bank slope stable.
*** Susceptibility do landslide.
R. Árvore, Viçosa-MG, v.29, n.2, p.327-336, 2005
riverbanks. Few shrubs and vegetable crop fields, which
are the predominant vegetation cover present in the
studied sites A and B, respectively, did not provide
enough protection to avoid erosion, thus the bank
is highly unstable and susceptible to erosion. This
was mainly related to sandy composition, low vegetation
cover and closeness to talweg.
The fast and progressive bank erosion process
mostly occurs when waves hit the unprotected riverbanks;
expose the root systems and eventually causing trees
to fall into the stream. Montrichardia linifera can
minimize this serious environmental problem in the
lower São Francisco River basin, and should be listed
in re-vegetation plans for this area, since it is easily
adapted to wetlands, propagates rapidly and is recognized
as a colonizer species. Additionally, wet meadow riparian
vegetation, here represented by Eleocharis elegans,
is another good example. Its roots appear to increase
bank strength by reinforcing soils (MICHELI and
KIRCHNER, 2002).
There is a strong and urgent need to restorate
the riparian zone with native or exotic plant species
that have a fast vegetative development, in order to
reduce riverbank erosion. Nevertheless, the preservation
of riparian remnants is vital because they produce source
of plant seeds, provide home for pollinators and dispersal
agents, and contribute enormously to the recovery
of the riparian zone.
Species that yield fruits, flowers for honey
production and medicines could be planted in the Lower
São Francisco to stimulate the landholder’s involvement
in the restoration process, and recover its biodiversity.
4- ACKNOWLEDGMENTS
We are Thankful to Professor Gilvane Viana for
field and laboratory assistance, to Mrs. Esther Alsum,
Mr. Francisco Arriaga and Prof. Joy Zedler for their
comments on an earlier draft.
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